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Full text of "Chemical exchange as a versatile isotope separation process"



UNITED STATES ATOMIC ENERGY COMMISSION 

Y-683 

CHEMICAL EXCHANGE AS A VERSATILE 
ISOTOPE SEPARATION PROCESS 



By 

G. H. Clewett 







November 7, 1950 

Oak Ridge National Laboratory, Y-12 Area 

' . '■■.■ Q r 
nXr.l IMENTS — 




\ L Us^EPOSiTORY 



Technical Information Sorvico, Oak Ridgo, Tonnottoo 



CHEMISTRY 



PRINTED IN U.S.A. 
PRICE 10 CENTS 



AEC. Oak Ridge, Term., 3-2 1-5 1-550- W-772 



CHEMICAL EXCHANGE AS A VERSATILE ISOTOPE SEPARATION PROCESS* 
By G. H. Clewett 



The successful large-scale separation of the uranium isotopes by two entirely different methods 
has led to an acceptance of isotope separation as an industrial process. The highly successful gaseous 
diffusion process has taken its place as a routine operation. At the same time the electromagnetic 
process has been demonstrating its versatility by supplying separated stable isotopes of nearly all 
existing kinds for research purposes. Various studies have shown that certain separated stable 
isotopes have properties of unusual value in nuclear science and technology. It is not unreasonable 
to believe that a day may come when separated isotopes of many elements will be available in bulk 
quantities for use in reactor construction and associated projects as well as for laboratory research. 
Thus isotope-separation processes may be destined to play an even greater role in the future develop- 
ment of nuclear energy than they played in the past. To bring about such a state, it will certainly be 
necessary to be concerned with costs and to develop those isotope-separation processes which are 
most efficient. 

For the lighter elements, the chemical-exchange method introduced and developed by Urey is 
generally accepted as being one of the most efficient. The close approach to thermodynamic equi- 
librium achieved in chemical-exchange processes with resultant minimal expenditure of energy at 
each stage leads to highly efficient low-cost production. 1 This is true if a suitable isotopic-exchange 
reaction can be found for the particular element in question. This necessity of searching for suitable 
reactions for each element prevents the chemical-exchange method from even approaching the versa- 
tility of the electromagnetic process. It arises, of course, from the heterogeneity of the chemical 
properties of the various elements. However, if the chemical and chemical-engineering requirements 
to be met if a successful process is to emerge are examined and the fields of knowledge which are 
involved are noted, it will be seen that the progress of research in these fields is such as to make the 
job continually less difficult. In fact, a condition is approached where it is possible to visualize the 
chemical-exchange process as having a high degree of versatility. In order to illustrate this, the 
following criteria have been reviewed. 

The specifications to be met by a suitable chemical-exchange system can be grouped into three 
chemical requirements and three engineering requirements. Reference to specific features of one of 
Urey's very well known and highly successful separation processes as these six points are listed 
will serve to clarify each in turn. The enrichment of N" by exchange between NH3 and NH provides 
an excellent example for this purpose. 2 

CHEMICAL CRITERIA FOR A SUCCESSFUL PLANT 

The three chemical criteria may be expressed as follows: 
1. The element must be distributed between two phases 



NH 3 (gas)-NH 4 (liquid) 



*Work performed under Contract No. W-7405-eng-26. 



Y-683 



Y-683 
2.' Rapid isotopic exchange must take place between the chemical forms in the two phases 

N 14 H 3 + N 15 ^ — N 15 H 3 + N 14 ^ 
3. The equilibrium constant of the isotopic exchange reaction must be other than unity 
, JNl5H 3 ] [N"H 4 + ] 



[n 14 « 3 ] [n 15 h 4 + ] 



1.035 at 298°K 



The reason for the stipulation of the two phases is rather obvious, but the rule can be broken. 
Thus, at least one successful example of a complete single-phase system is known. Bernstein and 
Taylor 3 were able to obtain enrichment of carbon 13 by use of the single-phase exchange 

c 13 + c 12 2 =** C 12 + C 13 2 

These workers were able to move the two species countercurrently by the use of a thermal-diffusion 
column. Since this is not a very efficient means of obtaining countercurrent flow, it is apparent that 
a two-phase system is preferable wherein simple pumps can be used. Immiscible pairs which might 
be used are shown in Table 1 . 

Table 1 

1. Gas-liquid 4. Liquid-solid 

2. Gas-solid 5. Solid-solid 

3. Liquid-liquid 

Almost all the reported successful chemical-separation processes have consisted of gas- liquid 
systems, and this type appears to be superior to all others. Examples of these are shown in Table 2. 



Table 2 



Product 


Gas phase 


c 13 


HCN 


c 13 


co 2 


N 15 


NH 3 


S 34 


S0 2 



Liquid phase 

(aq. compds) Reference 

CN" 4, 5 

HCO3 6 



NH+ 2 

*3 



HSOq 7, 



No clear-cut demonstration of a gas-solid system has been reported, although preferential 
adsorption of heavy-water vapor on carbon has been proposed as an isotope-separation method. 9 
Something of this type might be possible, using fluidization techniques, if the solid particles could be 
made small enough for rapid isotopic exchange to take place. 

There appears to be no reason why a liquid-liquid system should not be satisfactory, yet only one 
example has appeared — the enrichment of *>Li by exchange between lithium amalgam and an organic 
solution of a lithium salt. 10 

Semisuccessful liquid-solid systems have been reported, such as zeolite and ion-exchange resin 
separations of the isotopes of potassium and lithium. 11 However, these were all inherently batch proc- 
esses and are not amenable to development into continuous processes. 

Solid-solid systems are completely unlikely. 

The best possibilities are the two pairs, gas-liquid and liquid-liquid systems. Certainly, wherever 
possible, it would be desirable to have a gas-liquid system. Generally, however, only the nonmetallic 
elements provide suitable gaseous species, which leaves the necessity of considering a liquid-liquid 



Y-683 I 

system in most cases. It would appear then that the liquid-liquid type might be regarded as the most 
versatile. 

At this point it may be worth while to examine the third criterion, i.e., that the equilibrium con- 
stant for the isotopic-exchange reaction must be other than unity. Urey 12 ' 13 and others' 4 have shown 
how these constants may be calculated, and some degree of qualitative familiarity with the method is 
quite helpful in understanding which chemical equilibria lead to the largest separation factors. 
Bigeleisen and Mayer 14 devised two relatively simple formulas for calculating equilibrium constants. 
They point out several simplifying cancellations which take place in calculating ratios of partition 
functions for isotopic equilibria. Since the translational and rotational partition functions are classi- 
cal at room temperature in all cases except for hydrogen, the concern is solely with the vibrational 
partition function. The most general of the two formulas mentioned above is* 

|-f = 1 ♦liGd'i) Ai^i 

where G = 2~*V-1 

hv 

" = £t" 

Ai/ = change in v upon isotopic substitution. 

The second formula is for polyatomic symmetrical molecules containing isotopes of a heavy 
element. 



zrf = 1 



m 2 

U. n 



24 M 



2 1 



where 



hVj 
U, = -r=; and V, is the totally symmetric, or "breathing frequency" 

AM = difference in mass between the isotopes of the heavy element 
m = atomic weight of atoms bonded to the central heavy element 
M = mass of heavy element 
n = number of atoms bonded to the central heavy element 



Now, let us examine the ratio of partition functions for some isotopic chlorine molecules. 

1/2 



Mol. 
ratio: 



CI 



37 



1.0074 



ci 37 o 



ci 35 c. 



1.0313 



ci 35 o- 



1.0478 



37 - 

CI o„ 

4 

35 - 

CIO, 
4 

1.0847 



*Bigeleisen and Mayer carry the simplification further and obtain 

s y A (Ui )2 

ir f = 1+ A—ir- 



as a very rough approximation. 



4 Y-683 

Thus the equilibrium constants for the following isotopic-exchange reactions would be 

1/2 ClJ 7 + Cl35o 2 ^ 1/2 elf + C1 37 2 K = ijjgg = ^ 

l/2Clf + Cl3 5 03^1/2Cl 35 + Cl3V - K = ^ = 1.040 

1/2 Cl" + C1 35 0~ ^ 1/2 CI 35 ♦ C1 37 0~ K = ^jj|g = 1.077 

Urey 13 has pointed out that these are progressively larger with added oxygens because of the 
increased number of vibrational degrees of freedom and the approximate constancy of the vibrational 
frequencies of all the oxygen compounds of chlorine. That this is not always so is demonstrated by the 
examples chosen by Bigeleisen and Mayer 14 

28 r . o;30 r --^o;30iT c;28v-.- ,r 1-111 



Si 28 F 4 + Si 30 F6~=iSi 30 F 4 + Si 28 Fg 



K = no9^- 002 



Sn 12 C l 4 + Sn" 8 Ci: =* Sn 118 Cl 4 + Sn^d! K = |^|M = 1.00025 

D ^ D l.UUZOl 

Here a considerable cancellation effect is observed because the bonds have become weaker in 
the octahedral ion than in the tetrahedral ion, and the total restoring force is approximately unchanged. 
Other examples are available, but these allow a qualitative rule to be formulated for choosing suitable 
isotopic-exchange reactions. In order to obtain a large separation effect, it is evident that the element 
in question should exist in one phase unbonded or with only a few weak bonds, and in the other phase it 
should be bonded with as many bonds as possible, and these bonds should be strong. 

When the second chemical requirement of rapid isotopic exchange is examined, some degree of 
incompatibility is found between the various criteria. The species desired in one phase with many 
strong bonds is not likely to undergo rapid isotopic exchange with the free element, the ion, or a 
loosely bonded molecule. If the element is a metal, then one of the first choices of a pair of dissimilar 
forms is the metal ion in aqueous solution in equilibrium with a chelate complex or other complex of 
the metal in an immiscible organic solvent. Such coordination entities supply the many strong bonds 
which lead to a large separative effect, but these bonds are usually considered to be covalent, with 
resultant negligible exchange. However, if the presence or absence of exchange is accepted as a 
criterion of bond type, then it must be concluded that covalent bonds are not universally present in such 
coordination entities since there are numerous examples in which very rapid isotopic exchange takes 
place. The status of chemical knowledge of the structure of coordination compounds has been briefly 
summarized recently by Fernelius, 15 and his list of exchange reactions involving coordination com- 
pounds contains some which are described as very fast. 

Since the success or failure of the Szilard-Chalmers method of producing concentrated radioactive 
species is intimately related to ease of exchange, a study of some compounds which are not amenable 
to this treatment is helpful. Fernelius 15 lists a few compounds which apparently exhibit exchange, 
since the Szilard-Chalmers method was unsuccessful with each. 



Y-683 



Table 3 



Compound 



Reference 



Magnesium 

Mg ++ with Mg(8-hydroxyquinolinate)2 
(aqueous E + OH) 
Zinc 

Zn (pyridine)2 (OAc)2 with 
Zn acetylacetonate 
Zn acetylacetone-ethylenediamine 
Zn benzoylacetonate ammoniate 
Zn nicotinyl acetonate 
Zn (pyridine) 2 (SCN) 2 
Mercury 

CN~ with Hg(CN) 4 (pH 10) 
Manganese „ 

Mn ++ with Mn(C 2 4 )3 

Ir0n -4 -3 

Fe(CN) 6 with Fe(CN) 6 

Nickel 

CN~ with Ni(CN) 4 

Ni ++ with Ni (salicylaldehyde)3 

Ni ++ with Ni (ethylene diamine^ 

Ni with Ni (salicylaldoximo)3 

Ni with Ni (salicylaldimino)„ 
Platinum 

Br" with PtBr 4 ~ and PrBrg" 

Br in cis-[Pt(NH3) 2 Br 2 l with [PtBr 4 ]~~ 

Br in [PtBrg]"" with [PtBr 4 ]" 
Copper 

Cu ++ with Cu (acetylacetonate) 2 in CHCI3 

Cu + ^ with Cu derivations of salicylaldehyde 
and related compounds 



16, 17 



18 



19 

20 

21 

19 
22 
22 
22 
22 

23, 24 
23 
23 

16 
25 



Table 4 — Compounds Not Amenable to Szilard-Chalmers Effect 



Compound 



Reference 



Zinc 

Zn (acetylacetonate) 2 
Scandium 

Sc (acetylacetonate>3 
Vanadium 

V 2 C»3 (8-hydroxyquinoline) 4 

V(cupferron)g 
Uranium 

U0 2 (benzoylacetonate)2 
Manganese 

Mn (acetylacetonate)3 

Mn (benzoylacetonate) 2 



26 
27 



29 
30 



6 Y-683 

There seems to be no marked inconsistency between the conclusions from these experiments 
regarding bond type and the conclusions from other studies such as magnetic susceptibility measure- 
ments and experiments which differentiate between the planar configuration of covalent dsp^ bonds and 
the close-packed or tetrahedral arrangement of ions. Some apparent anomalies can be explained by a 
difference in bond type between the solid compound and a solution of the compound. In other cases 
certain solvents seem to convert part or all of the covalent molecules into complexes of ionic bonds, 
thus allowing exchange to take place. The point to be noted is that significant advances are being made 
in systematizing the knowledge of the structure of coordination compounds and, specifically, the condi- 
tions required for isotopic exchange. 

The application of this widening knowledge of complex compounds to isotopic equilibria in a 
quantitative way is some distance away as yet. It has been shown that even an approximate calculation 
of these equilibrium constants requires a knowledge of the vibrational frequencies arising from bonding 
of the element in question, and in most cases the shift in frequency upon isotopic substitution must also 
be known. If these frequencies are unknown and estimates are to be made, then it is, of course, very 
important to choose the proper atomic model. It will be remembered that the aim is to equilibrate some 
complex compound or ion of the isotopic element with some simple compound or ion. It would appear 
that the information about vibrational frequencies would not be difficult to obtain for the simple species 
in any case. However, where the element in question is a metal, the simple species will most likely 
be the simple positive ion. It appears that the water of hydration of such metal ions profoundly affects 
the vibrational partition function, and yet there is no measure of the frequencies of vibration of the 
metal-oxygen bonds in such hydrates, if, indeed, these frequencies have any physical meaning. 

It appears that they are completely absent in raman and infrared spectra. Bigeleisen 31 offers the 
explanation that perhaps the rate of exchange of water molecules or oxygen atoms about such a metal 
ion is of the same order of magnitude as the vibrational frequencies which might otherwise be observed. 

At any rate, it appears that the presence of water of hydration on these simple metal ions intro- 
duces an unknown factor in the problem of calculating isotopic equilibria. On the other hand, it may be 
of some academic interest that an experimental determination of the isotopic equilibrium factor for 
suitable individual cases provides an indirect method of learning something about the strength of these 
ion dipole bonds. Suppose, for example, the equilibrium 

++ ++ 

X A +y AC 2 Y A +X AC 2 

where A represents a divalent metallic ion, AC 2 represents an extractable complex, and the super- 
scripts represent two different isotopes of the element A. Suppose further that all vibrational fre- 
quencies are known for AC2 and that the equilibrium constant for this exchange reaction is known. It 
can be seen that through the use of the formulas of Bigeleisen and Mayer, the usual calculation can 
be reversed, and a numerical result can be obtained for a hypothetical symmetrical vibrational fre- 
quency for the hydrated ion. The accuracy of such a calculation is entirely unknown. 

It is apparent that the position as regards the versatility of quantitative calculations of isotopic- 
exchange constants is not a strong one. However, the methods of experimentally measuring these 
constants are straightforward even though rather tedious, so that the chemical-exchange method of 
separating isotopes is very little less versatile because of this difficulty in calculating the single- 
stage factor. 

From a chemistry standpoint, if a particular system satisfies the three rules, (a) distribution 
between two phases, (b) rapid isotopic exchange, (c) equilibrium constant other than unity, then it is 
ready for engineering development. 

ENGINEERING CRITERIA FOR A SUCCESSFUL PLANT 

Consider the development problems to be met in applying any exchange system. For the success- 
ful application of an isotopic-equilibrium reaction, certain conditions must be met which are more of 
the nature of chemical-engineering principles. There are various ways of expressing these require- 
ments, but for the present purposes they may be presented as follows. 



Y-683 7 

1. The two immiscible phases of the chemical-exchange system must be efficiently contacted as 
countercurrent streams. 

2. The apparatus must have low holdup and high throughput. 

3. Means for achieving total reflux at the top and bottom of the plant must be provided. 
When the first two points are considered together, the various means available for efficiently 

contacting two phases are discussed briefly below. This is where the real advantage of having a 
system which involves one gas and one liquid phase becomes apparent. That is, a simple packed 
column suitable for distillation provides a means of contacting these two phases efficiently with very 
short stage height. Furthermore, such distillation columns have been studied extensively in all sizes 
and pose no great problem in equipment design. However, as noted earlier, very often it will be 
impossible to devise a system having one gas phase, and probably liquid-liquid systems must be dealt 
with in most cases. When two liquids are contacted in an ordinary packed column, the stage heights 
are usually much greater than those observed with gas-liquid systems. That this should be of concern 
in no small degree will be manifested if a simple mathematical function in plant design is examined, 
namely, the time to reach equilibrium. 

In most distillation processes the single-stage factors are so large that the entire plant reaches a 
steady state or equilibrium condition almost as soon as it reaches thermal equilibrium. With an 
isotope -separation plant, the factor is usually so small and the plant is so long in terms of number of 
stages that there is a considerable time lag in starting up while the total plant production must go into 
building up the inventory of enriched material throughout the plant before any product may be with- 
drawn. The time to reach such a steady state is called the "time to reach equilibrium." Since it is 
dependent upon the rate of production as well as the size of the plant, it provides a simple measure of 
plant efficiency. The function is of the following form 

T = -^ *(No,N) 

where h = processing time per stage 

E = a-1 

4>(No,N) = function of No and N, which are mole ratio of desired isotope to undesired 
in product and feed, respectively 

The product and feed level are usually fixed. The single-stage separation factor is also fixed for 
any one system, but since it enters as a square term here, it simply points up further the importance 
of having a large separation factor. The main concern then is with the processing time per stage. If 
the rate of exchange of the isotopic reaction is very rapid, the processing time per stage becomes a 
function of the ratio of holdup per stage to throughput or interstage flow. Thus, in engineering an 
isotope-separation plant it is very important to achieve a short-stage height with high throughput. 

These same features are highly desirable in any plant using a liquid-liquid process, although not 
so critical in most, and continual progress is being made in devising new and improved equipment for 
this purpose. Besides various types of packed columns, there are spinner columns, 32 centrifugal 
separators, 33 as well as simple mixer settlers. Most engineers are familiar with these and many other 
contacting devices. The development of any design which achieves a significant decrease in the stage 
height or the ratio of holdup to flow in each stage can mean the promotion to complete feasibility of 
many otherwise borderline or impractical processes. 

The final criterion to be met, of achieving reflux at top and bottom of the plant, is not entirely 
an engineering problem. First of all, it is a chemical problem of converting the element in question 
from one chemical form to another. Here again, Urey's process for enriching N" provides an 
excellent example. The nitrogen, present as ammonium ion in the liquid phase, is converted to 
ammonia gas by treatment with caustic. The ammonia gas then travels back up the column to the top 
where it can then be reconverted to ammonium ion with acid. The net result of these chemical proc- 
esses is the neutralization of an acid with a base to produce a salt. Benedict 1 has pointed out that 



8 Y-683 

this net process and the acid and caustic chemicals used correspond to the power costs or energy 
costs in other types of separation plants. Because of the large reflux ratio, or ratio of interstage flow 
to product flow required in an isotope-separation plant, large quantities of chemicals are required 
usually in this reflux operation. Dependent upon the chemistry involved, equipment must be devised 
for each different process to accomplish this reflux. It must be done quantitatively with a minimum of 
holdup. 

Since the operating principle of each reflux mechanism is so dependent upon the chemistry of the 
system itself, very few generalizations are possible. Sometimes the chemistry of a particular system 
is such as to make it difficult if not impossible to attain this satisfactorily. For these cases it is 
important to note that a means of obviating the need for reflux has been proposed which is based upon 
the temperature coefficient of the separation factor. 34 The equilibrium constant for an isotopic- 
exchange reaction usually varies with temperature in some such manner as shown in Fig. 3. By 
suitable selection of Tj and T£, two towers can be used, a hot tower and a cold tower, operating with 
two different separation factors. Figure 4 shows how these towers are then connected. If the large 
factor of the cold tower favors the incoming stream at the top, then the smaller factor of the hot tower 
favors this same stream somewhat less as it emerges from the bottom of the hot tower. Thus, we have 
a build-up of desirable component between the two towers as shown in this diagram. The hot tower acts 
somewhat as a reflux mechanism since it prevents the exit from the system of desirable component 
by means of its smaller separation factor. Since this eliminates the need for large amounts of chemi- 
cals in the ordinary type reflux device, it might be concluded that this dual-temperature method would 
have somewhat of an advantage. However, this ease of reflux is counterbalanced more or less by the 
fact that a much larger plant must be built and operated because of the much lower net factor using 
the dual-temperature process which leads to a larger number of stages. Expressed graphically on a 
McCabe-Thiele diagram, Fig. 5, it is easy to see that many more stages are required. 

These then are the various criteria for successful application of chemical exchange to the 
separation of isotopes. It is believed that the advances now being made in the fields of knowledge 
mentioned above are such as to materially extend the applicability of this method. 

REFERENCES 

1. M. Benedict, Trans. Am. Inst. Chem. Engrs., 43: 41-60 (1947). 

2. H. G. Thode and H. C. Urey, J. Chem. Phys., 7: 34-39 (1939). 

3. R. B. Bernstein and T. I. Taylor, J. Chem. Phys., 16: 903 (1948). 

4. I. Roberts, H. G. Thode, and H. C. Urey, J. Chem. Phys., 7: 137 (1939). 

5. C. A. Hutchinson, D. W. Stewart, and H. C. Urey, J. Chem. Phys., 8: 532 (1940). 

6. A. F. Reid and H. C. Urey, J. Chem. Phys., 11: 403 (1943). 

7. H. C. Thode, R. L. Graham, and J. A. Ziegler, Can. J. Research, (B) 23: 40-47 (1945). 

8. D. W. Stewart and K. Cohen, J. Chem. Phys., 8: 904 (1940). 

9. D. F. Stedman, National Research Council, Canada, unclassified report C50-49S. 

10. G. N. Lewis and R. T. MacDonald, J. Am. Chem. Soc, 58: 2519 (1936). 

11. T. I. Taylor and H. C. Urey, J. Chem. Phys., 6: 428 (1938). 

12. H. C. Urey and L. J. Greiff, J. Am. Chem. Soc, 57: 321 (1935). 

13. H. C. Urey, J. Chem. Soc, 562 (1947). 

14. J. Bigeleisen and M. Mayer, J. Chem. Phys., 15: 261 (1947). 

15. W. C. Fernelius, Record Chem. Progress, Winter 1950. 

16. S. Ruben, G. T. Seaborg, and J. W. Kennedy, J. Applied Phys., 12: 308 (1941). 

17. S. Ruben, M. D. Kamen, M. B. Allen, and P. Nahinsky, J. Am. Chem. Soc, 64: 2297 (1942). 

18. L. Leventhal and C. S. Garner, J. Am. Chem. Soc, 71: 371 (1949). 

19. A. W. Adamson, J. P. Welker, and M. Volpe, San Francisco Meeting A.C.S., Apr. 1, 1949. 

20. M. J. Polessar, J. Am. Chem. Soc, 58: 1372 (1936). 

21. R. C. Thompson, J. Am. Chem. Soc, 70: 1045 (1948). 

22. J. E. Johnson and N. F. Hall, J. Am. Chem. Soc, 70: 2344 (1948). 



Y-683 

23. A. A. Grinberg, Bull. acad. sci. U.R.S.S., Ser. phys., 4: 342 (1940); C.A., 35: 3895 (1941). 

24. A. A. Grinberg and F. M. Filinov, Compt. rend. acad. sci. U.R.S.S., 23: 1912 (1939); C.A., 34: 
1246 (1940). 

25. R. B. Duffield and M. Calvin, J. Am. Chem. Soc, 68: 557 (1946). 

26. J. W. Kennedy, G. T. Seaborg, and E. Segre, Phys. Rev. 56: 1097 (1939). 

27. J. W. Kennedy, reported by H. Walke, Phys. Rev., 57: 166 (1940). 

28. P. Sue and T. Yuasa, J. chim. phys., 41: 160 (1944). 

29. K. Starke, Naturwissenschaften, 30: 107, 577-582 (1942). 

30. U. Drehmann, Z. physik. Chem., B53: 227 (1943). 

31. Bigeleisen, verbal discussion. 

32. W. O. Ney, Jr., and H. L. Lochte, Ind. Eng. Chem., 33: 825 (1941). 

33. Podbielniak Industrial Research and Engineering Laboratories, Chicago. 

34. Dual Temperature Process, MDDC-891. 



10 



Y-683 



NH 4 N0 3 — 



^ * NH 3 



NaOH 




"1 



NH 3 
GENERATOR 



r 



Fig. l—N 1 ^ (gas) + N 1 ^ (sol.) ^1%^ (gas) + 
N 1 !^ (sol.) [h. G. Thode and H. C. Urey, J. Chem. 
Phys., 7: 3^ (1939)]. 



Y-683 



11 



co 2 +co - 




I iCOHCO 




Fig. 2— C 12 2 (gas) + C^O (gas) ^ C^Og (gas) + 
C 12 (gas) [r. B. Bernstein and T. I. Taylor, J. 
Chem. Phys., l6: 903 (19^8)]. 



12 



Y-683 



a 




.000 



TEMPERATURE — 



Fig. 3 - -Variation of the equilibrium constant for an isotopic-exchange 
reaction with temperature. 



Y-683 



13 



COLD 



i i 
i i. 



~l 
i 

.J 



HOT 



Fig. k — Diagram of hot and cold towers connected. 



Ik 



Y-683 




Fig. 5 — McCabe-Thiele diagram. 



END OF DOCUMENT 



UNIVERSITY OF FLORIDA 



3 1262 08909 0269